Greenland is
melting about four times faster than it was in 2003, a new study published
Monday in the Proceedings
of the National Academy of Sciences found, a discovery with
frightening implications for the pace and extent of future sea level rise.
"We're going to see
faster and faster sea level rise for the foreseeable future," study lead
author and Ohio State University geodynamics professor Dr. Michael Bevis said
in a press release. "Once you hit that tipping point, the
only question is: How severe does it get?"
The study comes a week
after another study found that ice melt in Antarctica had
increased sixfold in the past 40 years and included consistent loss from East
Antarctica, a region previously believed to be more stable.
The Greenland study also found
that ice melt was coming from an unexpected place: Greenland's southwest
region, which is not home to iceberg-calving glaciers like the more studied
southeast and northwest. But the most consistent ice loss between 2003 and 2012
came from ice melting directly from this understudied region into the ocean.
"We knew we had one big
problem with increasing rates of ice discharge by some large outlet
glaciers," Bevis said. "But now we recognize a second serious
problem: Increasingly, large amounts of ice mass are going to leave as
meltwater, as rivers that flow into the sea."
The paper found that the
region "will become a major contributor to sea level rise" within two
decades, The New York Times reported.
The researchers used data from
Gravity Recovery and Climate Experiment (GRACE), twin satellites launched by
Germany and NASA in 2002 to monitor ice loss from Greenland, as well as from
GPS stations. They found that between 2002 and 2016, Greenland lost 280
gigatons of ice each year, adding 0.03 inches of water to the world's oceans annually.
Researchers did note a pause
in melting around 2013, which coincided with a reversal in the North Atlantic
Oscillation, which brings warmer air to Greenland periodically. However, Bevis
told The New York Times that the pause is actually a reason for concern.
Cyclical patterns of warmer and cooler temperatures did not usually impact
Greenland so dramatically. If the base-level temperature is now so warm that
natural warm cycles accelerate melting, but natural cool cycles only pause it,
then the ice sheet could be close to a "tipping point."
"One degree of warming in
the future will have way more impact than one degree of warming in the last
century," Bevis said.
But the authors of another study published in December 2018, which found
Greenland was melting at its fastest rate in 350 years, cautioned The New York
Times about the tipping point language.
"I take issue with using
'tipping point' to describe the accelerating mass loss Greenland is
experiencing," Woods Hole Oceanographic Institute scientist Dr. Sarah B.
Das said. "it makes it appear as if we have passed, or soon will pass, the
point of no return."
Her co-author Rowan University
glaciologist Dr. Luke D. Trusel agreed that there were still meaningful actions
humans could take to mitigate the loss.
"By limiting greenhouse
gas emissions we limit warming, and thus also limit how rapidly and intensely
Greenland affects our livelihoods through sea-level rise," he added.
"That, it seems, is our call to make."
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